| dc.contributor.author | Shank, Timothy M. | | |
Concept link
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| dc.date.accessioned | 2010-06-01T19:05:16Z | | | |
| dc.date.available | 2010-06-01T19:05:16Z | | | |
| dc.date.issued | 2010-03 | | | |
| dc.identifier.citation | Oceanography 23, 1 (2010): 104-105 | en_US | | |
| dc.identifier.uri | https://hdl.handle.net/1912/3551 | | | |
| dc.description | Author Posting. © Oceanography Society, 2010. This article is posted here by permission of Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 23, 1 (2010): 104-105. | en_US | | |
| dc.description.abstract | One of the longest seamount tracks in
the Atlantic Ocean was formed by the
Great Meteor or New England hotspot.
This more than 3000-km-long hotspot
track formed both the New England and
Corner Rise seamounts, with a pause
in volcanism 83 million years ago as
evidenced by the morphological gap
between chains. | en_US | | |
| dc.format.mimetype | application/pdf | | | |
| dc.language.iso | en_US | en_US | | |
| dc.publisher | Oceanography Society | en_US | | |
| dc.relation.uri | https://doi.org/10.5670/oceanog.2010.76 | | | |
| dc.title | New England and Corner Rise seamounts | en_US | | |
| dc.type | Article | en_US | | |
| dc.identifier.doi | 10.5670/oceanog.2010.76 | | | |
